Magnesioaubertite is a rare, water-soluble hydrous sulfate mineral typically found as a secondary mineral in mine dumps. It is easily identified by its characteristic pale blue color and its association with other secondary sulfate minerals in hyper-arid climates.
Is this magnesioaubertite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch magnesioaubertite with a known reference. Magnesioaubertite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: blue.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, crusts, efflorescences.
Often confused with
Magnesioaubertite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside magnesioaubertite
Minerals reported to co-occur with magnesioaubertite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MgAl(SO₄)₂Cl·14H₂O
- Mohs hardness
- 2-3
- Density
- 1.80 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals, crusts, efflorescences
- Cleavage
- On {010}, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral formed by the reaction of volcanic gases and aluminum-bearing rocks
Where rockhounds find magnesioaubertite
Classic worldwide localities
- Grotta de Faraglione and along the Baia de Levante, Vulcano, Lipari Islands, Italy
Field-hunting tip
Where it forms: A rare secondary mineral formed by the reaction of volcanic gases and aluminum-bearing rocks. If you start seeing alunogen, pickeringite, metasideronatrite in float, you are in the right ground. Typical habit: tabular crystals, crusts, efflorescences. Train your eye for that shape before scanning the outcrop.







